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• 61. Factsheet-Bardarbunga-140901

  -area. This corresponds to a magma discharge of 300 to 500 cubic metres per second. From observations yesterday evening, the volume of erupted lava is between 16 and 25 million cubic metres. The eruption has not created any ash-fall. Gas and steam rises to a couple of hundred metres above the eruption site, extending up to 1,200 m downwind. In connection with the FUTUREVOLC project, a gas /media/jar/Factsheet-Bardarbunga-140901.pdf

• 62. Factsheet-Bardarbunga-140904

  Low-wind speed condition is present in the area at the moment. Based on radar images the eruption cloud from today (composed of steam and volcanic gases) has not drifted far away and is mostly concentrated around the eruption site. Stations measuring SO2 further away from the eruption site are showing concentration below health and safety thresholds. Since this morning, the cloud reaches 6 /media/jar/Factsheet-Bardarbunga-140904.pdf

• 63. Factsheet_Bardarbunga_20141003

  accompanied by ash fall. Other scenarios cannot be excluded.  From the Icelandic Met Office: The Aviation Colour Code for Bardarbunga remains at ‘orange’.  From today, the Scientific Advisory Board will meet on Mondays, Wednesdays and Fridays. The next meeting will be held on Monday 6 October. The National Commissioner of the Icelandic Police, Department of Civil Protection and Emergency /media/jar/Factsheet_Bardarbunga_20141003.pdf

• 64. Grimsvotn_status_2011-05-24_IES_IMO

  and around it. The estimated height is below 5 km since clouds over the glacier were at 5-7 km and the plume did not reach above the cloud deck. The ash plume reached 8 km briefly at 14 UTC today, but decreased shortly there after. According to pilot reports the plume is visible at around 10 thousand feet, mostly light gray or brown in color, but pulsating to 15 thousand feet /media/jar/Grimsvotn_status_2011-05-24_IES_IMO.pdf

• 65. Dyngjujökull station

  and anemometer are not at a standard height (from the ground level) and the actual height will vary according to the snow conditions at the site. This abnormal setup affects the measurements and their comparison with observations made at standard exposure elsewhere. Extended periods of missing observations are also to be expected in the future, due to the harsh conditions and servicing problems /about-imo/news/dyngjujokull-1

• 66. Re-evaluation needed of the size of the hazard area

  field for about 300 meters distance and started a brush fire which can be seen on one of the two RÚV webcams. It is not clear what is causing these changes in volcanic activity, but changes in magma flow, the chemical composition of magma/gas, or possibly changes in the volcanic conduit cannot be ruled out. Considering these changes in activity, the size of the hazard area at the eruption site /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir

• 67. The eruption has come to an end

  of the caldera is at least 61 m but the rate was only 5 cm/day last week, compared to tens of centimetres earlier. The volume of the subsidence is 1.7 - 1.8 km³. Seismic activity in Bárðarbunga continues to diminish. Conditions on the eruptive site are still dangerous. Gas emissions at the eruption site and near the lava field are still life threatening. To the right is a view over the eruptive /about-imo/news/nr/3097

• 68. About the implementation

  on daily base. It must also pass accessibility validation to be of good use to blind people, sight impaired people and other disabled people. The main design decisions where to: Honor classical design principles that have evolved in recent years, e.g. using two and three column layout. Start by implementing simple and clear interface, accessible to all, for the main information. Add later /about-imo/the-web/implementation/

• 69. The volcano measured

  thickness is 10-12 meters and estimated volume of eruptive material 22-24 million cubic meters (only one fifth of Hekla 2000). Accordingly, the average flow rate has been approximately 15 cubic meters per second since the eruption began. The eruptive cone stands 82 m above previous ground level and the highest peak is 1067 m a.s.l. On their web-site, explanatory photographs can be found (pdf 1.1 Mb /about-imo/news/nr/1862

• 70. Magma splatters ejected

  of this phenomenon at IMO yet. Magma splatters have have accumulated on the crater's rim. Splatters of magma have also fallen on the ice around the crater and this gives rise to steam plumes. In spite of the ejected batches of liquid magma, no lava flow from the craters was detected. South of the eruptive site, the ash clouds reached 5-6 km hight. Eyjafjallajökull ash cloud - two days ago /about-imo/news/nr/1883